A multi-frequency receiver function inversion approach for crustal velocity structure

被引:12
作者
Li, Xuelei [1 ,2 ,3 ]
Li, Zhiwei [2 ]
Hao, Tianyao [1 ]
Wang, Sheng [1 ,3 ]
Xing, Jian [1 ,3 ]
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Beijing 100029, Peoples R China
[2] Chinese Acad Sci, Inst Geodesy & Geophys, State Key Lab Geodesy & Earths Dynam, Wuhan 430077, Peoples R China
[3] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
关键词
Receiver function; Multi-frequency; Global optimizing; Crustal velocity structure; Inversion; UPPERMOST MANTLE STRUCTURE; SURFACE-WAVE DISPERSION; STRUCTURE BENEATH; JOINT INVERSION; DHARWAR CRATON; DIFFERENTIAL EVOLUTION; SEISMIC EVIDENCE; TRANSITION ZONE; TOMOGRAPHY; ALGORITHM;
D O I
10.1016/j.cageo.2017.02.009
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
In order to constrain the crustal velocity structures better, we developed a new nonlinear inversion approach based on multi-frequency receiver function waveforms. With the global optimizing algorithm of Differential Evolution (DE), low-frequency receiver function waveforms can primarily constrain large-scale velocity structures, while high-frequency receiver function waveforms show the advantages in recovering small-scale velocity structures. Based on the synthetic tests with multi-frequency receiver function waveforms, the proposed approach can constrain both long- and short-wavelength characteristics of the crustal velocity structures simultaneously. Inversions with real data are also conducted for the seismic stations of KMNB in southeast China and HYB in Indian continent, where crustal structures have been well studied by former researchers. Comparisons of inverted velocity models from previous and our studies suggest good consistency, but better waveform fitness with fewer model parameters are achieved by our proposed approach. Comprehensive tests with synthetic and real data suggest that the proposed inversion approach with multi-frequency receiver function is effective and robust in inverting the crustal velocity structures.
引用
收藏
页码:45 / 55
页数:11
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